The Farmville granite of DeRatmiroff (1972) is herein elevated to formal lithodemic status as Farmville Metagranite of Opelika Complex. Unit replaces the here abandoned Bottle granite of Bentley and Neathery (1970). At the designated type locality in Lee Co., AL, unit is described as medium to coarse grained and well foliated by dimensionally aligned biotite and quartz. Reference localities 1.5 mi due west of Farmville Church and west of Auburn are representative of lesser deformed cores. Locally contains porphyroblasts of potassium feldspar and is commonly cut by narrow pegmatite veins. Numerous sills of the Farmville intrude the Auburn Gneiss and Loachapoka Schist. Synmetamorphic intrusion of the unit is indicated by 369+/-5 m.y. age (Rb-Sr isotopic data from Goldberg and Burnell, 1987) and later deformation by 295+/-4 m.y. age (Rb-Sr mineral isochron from Goldberg and Steltenpohl, 1988). Emplacement age, therefore, is Late Devonian (Acadian).

Source: GNU records (USGS DDS-6; Reston GNULEX).

Inner Piedmont is divided into two groups of rocks, Dadeville and Opelika Complexes (Bentley and Neathery, 1970), divided by Stonewall line. Dadeville Complex consists of Agricola Schist, Waresville Schist, Camp Hill Gneiss, Chattasofka Creek Gneiss, Ropes Creek Amphibolite, Waverly Gneiss, Simmons Crossroads metagranite, and various unnamed mafic and ultramafic intrusive rocks. Opelika Complex consists of Loachapoka Schist, Saugahatchee quartzite, and Auburn Gneiss and schist. Farmville Metagranite intrudes these units. Report includes geologic sketch map. [Although GNU review requested informal terms to be inverted, the final draft sent to GSA (with copy to GNU) showed that authors did not comply with request.]

Source: GNU records (USGS DDS-6; Reston GNULEX).

Recent geologic mapping, petrographic and geochemical studies, and some geochronological data of rocks called Lithonia Gneiss, Mount Arabia migmatite within Lithonia Gneiss around Mount Arabia, Odessadale Gneiss in central GA (R.L. Atkins, unpub. mapping), and Farmville Metagranite of Opelika Complex in eastern AL have shown that 1) they are part of the same complex unit, 2) that several textural varieties are common to all of them in outcrop, 3) that they all occupy the same structural or stratigraphic interval, 4) that they have approximately the same mineral and chemical compositions, and 5) that their ages range between about 380 to 360 Ma (Middle to Late Devonian). Because of uncertainties in Pb-U zircon age data, because Rb-Sr and K-Ar ages could have been affected by metamorphism, and because overall sampling has been limited, all the gneisses are assigned an Ordovician to Devonian age.

Source: GNU records (USGS DDS-6; Reston GNULEX).